[Reading Comprehension]
试题详情
文章:
| Line | Milankovitch proposed in the early twentieth |
| century that the ice ages were caused by variations | |
| in the Earths orbit around the Sun. For some time | |
| this theory was considered untestable, largely | |
| (5) | because there was no sufficiently precise |
| chronology of the ice ages with which the orbital | |
| variations could be matched. | |
| To establish such a chronology it is necessary to | |
| determine the relative amounts of land ice that | |
| (10) | existed at various times in the Earths past. A |
| recent discovery makes such a determination | |
| possible: relative land-ice volume for a given period | |
| can be deduced from the ratio of two oxygen | |
| isotopes, 16 and 18, found in ocean sediments. | |
| (15) | Almost all the oxygen in water is oxygen 16, but a |
| few molecules out of every thousand incorporate the | |
| heavier isotope 18. When an ice age begins, the | |
| continental ice sheets grow, steadily reducing the | |
| amount of water evaporated from the ocean that | |
| (20) | will eventually return to it. Because heavier |
| isotopes tend to be left behind when water | |
| evaporates from the ocean surfaces, the remaining | |
| ocean water becomes progressively enriched in | |
| oxygen 18. The degree of enrichment can be | |
| (25) | determined by analyzing ocean sediments of the |
| period, because these sediments are composed of | |
| calcium carbonate shells of marine organisms, | |
| shells that were constructed with oxygen atoms | |
| drawn from the surrounding ocean. The higher the | |
| (30) | ratio of oxygen 18 to oxygen 16 in a sedimentary |
| specimen, the more land ice there was when the | |
| sediment was laid down. | |
| As an indicator of shifts in the Earths climate, | |
| the isotope record has two advantages. First, it is a | |
| (35) | global record: there is remarkably little variation in |
| isotope ratios in sedimentary specimens taken from | |
| different continental locations. Second, it is a | |
| more continuous record than that taken from rocks | |
| on land. Because of these advantages, sedimentary | |
| (40) | evidence can be dated with sufficient accuracy |
| by radiometric methods to establish a precise | |
| chronology of the ice ages. The dated isotope | |
| record shows that the fluctuations in global ice | |
| volume over the past several hundred thousand | |
| (45) | years have a pattern: an ice age occurs roughly once |
| every 100,000 years. These data have established | |
| a strong connection between variations in the Earths | |
| orbit and the periodicity of the ice ages. | |
| However, it is important to note that other | |
| (50) | factors, such as volcanic particulates or variations |
| in the amount of sunlight received by the Earth, | |
| could potentially have affected the climate. The | |
| advantage of the Milankovitch theory is that it | |
| is testable; changes in the Earths orbit can be | |
| (55) | calculated and dated by applying Newtons laws of |
| gravity to progressively earlier configurations of the | |
| bodies in the solar system. Yet the lack of | |
| information about other possible factors affecting | |
| global climate does not make them unimportant. |
题目:
It can be inferred from the passage that calcium carbonate shells
选项:
A、are not as susceptible to deterioration as rocks
B、are less common in sediments formed during an ice age
C、are found only in areas that were once covered by land ice
D、contain radioactive material that can be used to determine a sediments isotopic composition
E、reflect the isotopic composition of the water at the time the shells were formed
答案:
E